If Puget Sound is Falling Down - Earthquake Studies

This story was originally written in 1994.clues about these earthquakes involves both
William Steele, the Seismology Lab Coordinator atpainstaking research and educated guesswork.
the University of Washington GeophysicsResearch has recently identified a Seattle fault
Program, has a son, Chris, who goes towhich generated a large quake between 1,000 to
elementary school. "He comes in sometimes and1,100 years ago. "There were landslides, and a
he loves to do stuff." It seems he'd recently puthuge seiche-when something big falls in the water,
a sticker on one of the lab's monitors, and hiscreating waves like tsunamis. Large block
father had some trouble accessing the equipment.landslides occurred in forests. Restoration Point on
"What an excuse!" Steele never did get into theBainbridge Island rose twenty feet from Puget
program he'd wanted to show me.Sound in seconds during that event."
December 4th of last year there was aBuildup from glacial ice sheets once covering the
magnitude 5.1 quake in Klamath Falls, Oregon.continent make it difficult to analyze shallow crust
Aftershocks were felt in Washington State. I hadfaults. But geologists are pretty sure there are
headed out to the UW in search of information ontwo major Seattle faults. The biggest one runs
recent earthquake activity in the Puget Soundfrom the north tip of Mercer Island through
region.Eastgate to the Kingdome, just north of West
"Oregon is relatively quiet next to Washington. ButSeattle. The other fault runs through White
this year, we've had an enormous amount ofCenter, parallel to the bigger one. In 1872, an
activity in Oregon, counter to past patterns."estimated 7.3 shallow quake caused what
Klamath Falls couldn't be noisier, said Steele, tickingseismologists call "felt reports" from observers,
off the numbers: September 4th, 5.9; Sept. 20th,the only evidence of some older quakes. Native
5.9, 5.0, 4.3; Dec. 4th, 5.1; and Christmas Day, 4.0,Americans tell legends about what must have
3.4.been some very sizeable earthquakes and
Most of our local activity in the Puget Soundtsunamis.
region is recorded by the UW's lab equipment.Nowadays, all the real-time telemetry (automatic
They have an emergency preparation computertransmission of data from a distant source to a
program called "Beat the Quake," hailing from thereceiving station) comes through in the back of
land of quakes, California, which has sufferedthe lab, where Steele poured me a cup of
through quite a lot of severe earthquake damageStarbucks coffee at their metal sink in a very
lately. That's the program Steele had troubleequipment-crowded space. "Relays 'zap' activity
running on his computer. Fortunately, the UW'senergy in nanoseconds to the lab. Before people in
Seismology Lab has far more emergencya region know what's going to hit them, we do."
preparedness information "so we don't have toThe helicorders monitor 23 stations on analog.
begin from ground zero" in the likely event of an"We focus on volcanoes. All stations, including the
earthquake. Steele is also the Public Informationones on helicorders, go onto the computer
Officer covering quakes through the UW. "Wesystem in the next room. The discriminator in the
have 135 seismic stations throughout Washingtonback takes FM carrier signals and separates them
and Oregon, currently operating, and we'refrom seismic signals, leaving an amplified seismic
expanding. We really cover a tremendously broadsignal. It goes to the front room, changing into
area."digital information the computer can read.
They locate quakes precisely, then determine the"If it picks up a 'jump' (a skip in the needle on the
magnitude (quantity of total energy released byhelicorder) on a station, it checks other stations
the quake), location (area affected by the quake),and records all data, whether there's a signal or
and epicenter (location on the surface directlynot. If it's a big quake, it does estimates of the
above the focus, or place where an earthquakemagnitude etc. via programs, beeps the people
originates.)(like Steele), and sends information to
They collect data about the geology of the regionseismologists around the region." Steele might
as well. "It's critical data. This lab is an educationalhear a "beep" anytime.
center for graduate students in geophysics." TheyAs I drank my coffee, Steele told me he was a
also educate citizens. School groups bring ingrad student, his life's partner works, and
students, and Steele speaks at civic organizations,together they support their family, renting a
encouraging people to take action and makehouse in Wallingford and raising two kids. "It's a
themselves safer from earthquakes.rewarding job, but...the rewards are not
Of course, the big question everyone asks is,monetary." Nonetheless, he feels treated as a
"When?"colleague by everyone, and has a good working
"We're not able to put down a date. It's morerelationship with all his "fellows at the lab."
complicated because three types of quakes occurAbout earthquake preparedness, Steele is
in the Puget Sound region. The most common areadamant. "The secret is not fear and loathing in
deep earthquakes.Seattle, and that we have to hide under our beds.
"Signals travel through the planet's crust,Let's get ready. Our schools need to get to the
sometimes all the way from the other side."point where we can withstand a 7.4 earthquake.
Events from anywhere show up on theirHow many little bodies do we need under bricks
helicorder sheets, making an analog, a 24-hourbefore we start spending some money?" Right
record, of every quake. For example, the Klamathnow, there are no definite laws enforcing
Falls quakes, which are very near California on theearthquake building codes, "if the building code
Oregon coast.years ago said you could pile bricks without
"We cover the Cascade Range, and have multiplemortar on top of each other."
stations on every volcano. We have a goodUnreinforced masonry creates structures that fall
station at Mt. Baker, adequate to cover theduring even moderate earthquakes. "The entire
region." Earthquakes around volcanoes are verywall of a school can fall down and kill students. A
common.brick that falls three stories doesn't slow down,"
The lab shares data with California for quakeshe said, referring to the death of a boy during the
occurring on the border of California and Oregon.1965 earthquake. Steele is certain such deaths are
"We're part of the Washington Regional Seismicpreventable.
Network." Steele showed me a map of PacificAt least six schools in Oregon have unreinforced
Northwest Seismicity, 1969-1991. There werestructures, bricks that can fall and fill a doorway,
huge blue clusters in Puget Sound. What areblocking the exit. "Retrofit them, or tear them
those, I asked. "Moderate, shallow, and deepdown and build another school. If a school has
quakes. The deep clusters are in the Puget Basin."been considered unsafe for a quake lately, they
Deep earthquakes, the ones you really tend tocan sell it, and it becomes a senior center. No laws
write home about, are the largest in magnitude asstop that. These buildings need to be brought up
measured on the Modified Mercalli Intensity Scale.to code or taken down. Deaths will happen unless
The values usually range from 1.0 (not felt) to 7.0we act. India just had a 6.8 quake...tens of
(extreme damage to buildings and land surfaces).thousands dead. There needs to be water and
They can go even higher, as they have in recentfood stored away to last 72 hours. You need to
deep quakes in Alaska.get under a table and ride it out; get down on the
Here's what's happening in Puget Sound: about 300ground, under something; check to see if you
kilometers or more out from the coast is wheresmell gas, and turn it off; electricity, too."
the deep quakes are generated. There's a ridgeYou should get to know your community
500 to 700 kilometers out called the Juan de Fucaresources, Steele said. And in case of severe
Ridge, and new material, new sea floor, is beingaftershocks, if you're in a building "you should wait
deposited all the time along it. It pushes the Juanuntil the shaking stops, and then get out." Lots of
de Fuca plate toward the North American platepeople are killed by falling debris while evacuating
underneath the Seattle area. The Juan de Fucabuildings.
plate moves an average of two inches a year,What does Steele see in the immediate future? "I
towards us, lifting the other plate.expect more of the same. Probably some quakes
A border zone locks it up, an interface betweengreater than 4.0 in the Puget Sound area. While
the two plates that stops the oceanic plate,we've been talking, there've been events in
making it subduct beneath us, forcing the oceanKlamath Falls,." As I write this, there are
plate down into the mantle of the Earth. Thisaftershocks east of the Dec. 4 "sequence"
boundary is called the Cascadia Subduction Zone,starting in Klamath Falls. "The question is, are we
and extends from the middle of Vancouver Islandgoing to recognize the danger and do something
in British Columbia down to Northern California.about it, or are we going to wait until we have an
The Earth's mantle lies beneath its brittle crust. It'sadequate death toll? I'd like to see a dedicated
semi-solid, due to tremendous heat and pressure.plan and some leadership from the state. It'll be a
"Our Cascade volcanoes are probably therelot of money."
because of plate subduction beneath us. The pushSteele said a colleague of his said it best: "The
deforms the crust and builds up tremendousnext great disaster will happen as soon as we
stresses. Right now, the coast of Washington isforget about the last one."
rising. It's bulging up." The oceanic plate is "coldWhat to do other than screaming your lungs
rock" and the shock of the two forces meetingout...fall down!
leads to deep earthquakes. Washington hasApparently, you may hear a very loud, building
recently experienced two large ones, in 1949 andsound before the frenzy begins. The below is
1965.from "How to Survive in Earthquake Country," a
A flyer from the lab states that roughly 1,000FEMA pamphlet. Find out about your risks, at
earthquakes per year are recorded in Washingtonhome, and in your workplace. Get more specifics
and Oregon. "Between one and two dozen offrom the American Red Cross, or FEMA.
these cause enough ground shaking to be felt byLearn what causes injuries: parts falling off building
residents. Most are in the Puget Sound region, andexteriors and interiors; flying pieces of broken
few cause any real damage. However, based onglass; overturning bookcases; unanchored water
the history of past damaging earthquakes and ourheaters; storage facilities; anything made of glass;
understanding of the geologic history of the Pacificfires from damaged gas lines; electric lines; wood
Northwest, we are certain that damagingstoves; chimneys; toxic fumes.
earthquakes (magnitude 6.0 or greater) will recurCreate emergency preparedness plans: find safe
in our area, although we have no way to predictspots in your home; identify escape routes; plan
whether this is more likely to be today, or yearstwo ways out of each room; pick two places to
from now." Steele thinks it will be soon.meet, outside your house and outside the
"In 1949, there was a severe earthquake inneighborhood if you can't return home; show
Olympia, 7.1. Eight people were killed and thereeveryone how to shut off water, gas and
was millions of dollars worth of property damage.electricity; practice your plans, now.
The quake was located 70 kilometers deep.Read "Your Family Disaster Plan," and "Emergency
"In 1965, there was a magnitude 6.5 quakePreparedness Checklist," which you can get from
between Seattle and Tacoma." Both earthquakesFEMA.
were felt as far away as Montana. But thereReduce earthquake hazards: evaluate your home;
were no aftershocks, as is usual during a deepstrap water heaters and gas appliances down;
quake. The infamous aftershocks, known to catchremember, stiff items snap; place heavy objects
people in the middle of recovering from a badon lower shelves; anchor everything heavy;
earthquake, happen during land-based shallowanchor hanging objects; support community
earthquakes. The ocean-based shocks occurredearthquake preparedness.
once, causing ground tremors that lasted severalBusinesses, schools, daycares, neighborhoods,
minutes. "The 1965 quake killed about five people,churches, clubs: hold workshops. Assemble a
and again there was millions of dollars of propertydisaster preparedness kit: store food, water,
damage." Other deep events, difficult to calculateclothes, a first aid kit, a radio, flashlights, and
from records of the times, occurred in 1882,batteries, good for 72 hours of use, in your car
1909, and 1939. "Every 35 years or so a 6.0+trunk, home, and office. For more details, consult
magnitude quake occurs beneath Puget Basin. Thethe FEMA brochure, "Your Family Disaster Supplies
whole region along the coast will shift at once.Kit."
When it finally builds up enough pressure to kickDuring/after an earthquake: stay calm; don't panic
up, it'll be a big one."or run. Earthquakes are usually preceded by loud
Eighty percent of the quakes on the planetsounds, so take quick action. You actually have
happen along the Pacific North West Rim, which isabout two seconds, so get ready for that
referred to as "The Ring of Fire" because of allearthquake now to protect yourself and others.
our volcanic activity. In 1964, one year before thisStay where you are: drop, cover and hold
area's last big event, south-central Alaskasomething solid, or take immediate cover under a
generated a monster 9.3 quake, shaking theheavy desk or table, in a doorway, hallway, or
ground for twenty minutes, generating tidalagainst inside walls. Turn away from glass. Keep
waves that decimated Seward's coast, affectedaway from chimneys, windows, tall bookcases,
34,000 square miles, and killed 143 people. Andand objects that might fall.
there's been recent large quakes in CapeEvacuate only after the shaking stops. Use the
Mendecino, California, and Parkfield, California,stairs, not the elevator. Remember, aftershocks
infamous for ground shaking, in 1992.may occur at any time. Listen to a radio or TV
Brian Atwater of the USGS (United Statesfor instructions. Outdoors: move away from
Geological Service) and the UW geologybuildings, trees, and utility wires. Sit on the ground
department has done studies along the coasts ofuntil the shaking stops. Flee inland immediately
Washington and Oregon. He's found a kind ofwhen near a coastline. Check for injuries. Do not
layered soil..."what he found...ghost forests killed bymove seriously injured people unless they're in
the last big quakes. Subduction zone materialdanger. Indoors: evacuate damaged buildings, as
covered by coarse black sand." A layer graduallyaftershocks could cause additional damage, or
turned into forest floor and then the sand layer.buildings can collapse.
"As bulging continues, coastline rises, and low-lyingDo not re-enter a building until it's declared safe
areas are flushed clean by salt water. Stressby responsible authorities. Don't use the telephone
released during the quake makes the coastlineexcept for emergencies; stay off the phone.
subside by seven or eight feet. It 'drops.' If you'reCheck for fires. Have a fire extinguisher, and
living at five feet above sea level, it's not a veryknow how to use it. Check utilities: gas, electric,
comfortable thing."and water lines may be broken. Gas: do not use
Earthquakes also generate large tsunamis, or tidalmatches, candles, open flames or electric
waves; the biggest ones, generated by largerswitches indoors, because of possible gas leaks. If
quakes, can rip up an entire coastline for miles,you smell gas, open windows, leave, and shut off
wiping out bridges, roads, and buildings. The reallythe main gas valve, which is usually outside.
great subduction zone quakes, 9.0 or more, onlyElectricity: if wiring is broken, shut off electricity at
occur about once a century on the face of thethe main switch. Don't touch anything near
planet. Strangely, a big quake may result in onlydowned or damaged lines. Water: if water pipes
about three-and-a-half minutes worth of strongare broken, shut off the supply at the main valve
ground shaking, which doesn't sound like much.outside. Use water from ice cubes, water heaters,
"One recent California quake was only seventeentoilet tanks (if they don't contain chemical
seconds of strong ground motion, a 7.1 quake. Acleaners). Clean up spills. Attend carefully to spills
7.0 quake releases the equivalent of 199,000 tonsof potentially harmful materials such as medicines,
of TNT in energy; a 9.0 releases 200 million tons,drugs, and household cleaners. Provide adequate
or 17,000 atomic bombs' worth of force.ventilation, as chemicals may combine to produce
"The difference between an 8 and a 9 is greatertoxic gas. Remember to assist others in need.
than the difference between a 2 and an 8,Finally, please remember to keep current on the
because of the logarithmic scale. The force"stats" regarding earthquakes, volcanoes and
increases exponentially. It gets 30 times greaterother natural disasters in your area, so you have
each time." I wondered if it ever goes up to 10.0.a pretty good idea what to do - in the likely
By carbon-14 dating organic matter in ground andevent you will have to suffer through one. And
sea levels, "scientists can determine approximatealso remember: it's not your fault. (Sorry about
dates for events going back 10,000 years." Findingthat, I couldn't resist the joke.